Características biogeoquímicas da interação atmosfera criosfera na Antártica ocidental

• Autor(a) principal: Silva, Marcio Cataldo Gomes da
• Data de Publicação: 2011
• Tipo de documento: Tese
• Idioma: por
• Título da fonte: Biblioteca Digital de Teses e Dissertações da UERJ
• Texto Completo: http://www.bdtd.uerj.br/handle/1/16132
• topic: Antarctica; Mmineral dust; Ice core; Atmospheric transport; Black carbon; Pyrosequencing; Antártica; Poeira mineral; Testemunho de gelo; Transporte atmosférico; Black carbon; Pirosequenciamento; CNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOFISICA

The antarctic ice cap stores paleoclimatological information within layers of snow and ice. Antarctic ice has revealed the higher resolution paleoclimactic database for the last 800 kyr. Atmospheric transport plays a fundamental role on the composition and sources of particulate matter found in the Antarctic ice. It has been related to several climatic processes that changes the quantity and quality of exogenous aerosols reaching Antarctica. Therefore, studies of the particulate matter deposits along the snow/ice layers may suggest changes on atmospheric transport patterns. This work, analyze two recent ice cores from two climatic distinct regions of the Antarctic continent. One retrieved from Detroit Plateau/Antarctic Peninsula (64°10′S/060°0′W), in which we have analyze Black Carbon (BC) deposition and variability along 20 meters of snow. BC found in the Antarctic Peninsula showed low concentrations (varing between 0,014 and 3,733ppb), comparable to the concentrations found on Arctic ice dated from before the industrial revolution period. Our results suggest that peaks of BC detected correspond, mostly, to biomass burning seasons in the South Hemisphere, not speficically from South America. The second one, of 40 m, was retrieved from Central-West Antarctica, Mont Johns (79o55′S/094º 23′W), in which we analyzed the mineral dust abundance thought M.E.V. E.D.X. technique. In this study we found negative trends in mineral dust (inferred from Fe, Ti and AlSi) deposition between 1967 and 2007, in contrast to similar works in Sub-antarctic regions. We demonstrate that this trend is a consequence of the persistent atmospheric isolation that encloses the Central and East Antarctic regions due to the increasing winds around Antarctica within this period. It has been documented that westerlies intensification reflect the upper atmosphere cooling above Central Antarctica caused by the stratospherical ozone layer depletion. As part of the polar site characterization, we additionally have performed sampling for microbiological purpose from distinct microenvironments at Patriot Hills (80°18′S/081°21′W). Samples were cultivated on R2 media and at the same time total DNA on samples was extracted and sent to a pyrosequencing analysis. Preliminary results show richness and diversity of bacterial species distributed on five phyla.